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首页> 外文期刊>Annales Geophysicae >A meteor head echo analysis algorithm for the lower VHF band
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A meteor head echo analysis algorithm for the lower VHF band

机译:较低VHF波段的流星头回波分析算法。

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We have developed an automated analysis scheme for meteor head echoobservations by the 46.5 MHz Middle and Upper atmosphere (MU) radar nearShigaraki, Japan (34.85° N, 136.10° E). The analysisprocedure computes meteoroid range, velocity and deceleration as functions oftime with unprecedented accuracy and precision. This is crucial forestimations of meteoroid mass and orbital parameters as well asinvestigations of the meteoroid-atmosphere interaction processes. In thispaper we present this analysis procedure in detail. The algorithms use acombination of single-pulse-Doppler, time-of-flight and pulse-to-pulse phasecorrelation measurements to determine the radial velocity to within a fewtens of metres per second with 3.12 ms time resolution. Equivalently, theprecision improvement is at least a factor of 20 compared to previoussingle-pulse measurements. Such a precision reveals that the decelerationincreases significantly during the intense part of a meteoroid's ablationprocess in the atmosphere. From each received pulse, the target range isdetermined to within a few tens of meters, or the order of a few hundredthsof the 900 m long range gates. This is achieved by transmitting a 13-bitBarker code oversampled by a factor of two at reception and using a novelrange interpolation technique. The meteoroid velocity vector is determinedfrom the estimated radial velocity by carefully taking the location of themeteor target and the angle from its trajectory to the radar beam intoaccount. The latter is determined from target range and bore axis offset. Wehave identified and solved the signal processing issue giving rise to thepeculiar signature in signal to noise ratio plots reported byGalindo et al. (2011), and show howto use the range interpolation technique to differentiate the effect ofsignal processing from physical processes.
机译:我们开发了一种自动流水线回声观测的分析方案,该方案是通过日本Shigaraki附近的46.5 MHz中高层大气(MU)雷达(北纬34.85°,东经136.10°)完成的。分析过程以前所未有的精度和精确度计算流星体的距离,速度和减速度作为时间的函数。这是流星体质量和轨道参数以及流星体-大气相互作用过程研究的重要基础。在本文中,我们详细介绍了此分析过程。该算法结合了单脉冲多普勒,飞行时间和脉冲与脉冲的相位相关性测量结果,以3.12 ms的时间分辨率将径向速度确定在每秒几十米的范围内。等效地,与以前的单脉冲测量相比,精度提高了至少20倍。这样的精确度表明,在大气中流星体消融过程的强烈过程中,减速度显着增加。根据每个接收到的脉冲,将目标范围确定为几十米以内,或者确定为900 m长距离门的百分之几。这是通过在接收时发送以2的因数过采样的13位Barker码并使用Novelrange内插技术来实现的。通过仔细考虑主观目标的位置以及从其轨迹到雷达波束的角度,从估计的径向速度确定流星体速度矢量。后者由目标范围和孔轴偏移确定。我们已经确定并解决了信号处理问题,该问题在Galindo等人报告的信噪比图中引起了特殊的签名。 (2011),并展示了如何使用范围插值技术来区分信号处理和物理过程的效果。

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